An igneous intrusion is a body of igneous rock that forms when magma from beneath the Earth's surface cools and solidifies within pre-existing rock layers. These intrusions can vary in size and shape, including features like dikes, sills, and plutons. They play a crucial role in understanding geological processes and the history of the Earth's crust, as they can provide insights into the composition and behavior of the magma. Additionally, igneous intrusions can influence the surrounding rock by causing metamorphism or altering mineral compositions.
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